Biblio
Finite element modeling of ultrasound measurement systems for gas. Comparison with experiments in air. Journal of the Acoustical Society of America 144, (2018). Abstract
A model of solar coronal heating by classical inverse bremsstrahlung and generation of the solar wind. Astrophysical Journal 412, (1993).
Arctic Clouds and Surface Radiation – a critical comparison of satellite retrievals and the ERA-Interim reanalysis. Atmospheric Chemistry and Physics (ACP) 12, (2012).
Waveform classification of airborne synthetic aperture radar altimeter over Arctic sea ice. The Cryosphere 7, (2013).
Uncertainties in Arctic sea ice thickness and volume: new estimates and implications for trends. The Cryosphere 8, (2014).
Adaptively varying-coefficient spatiotemporal models. Journal of the Royal Statistical Society: Series B (Statistical Methodology) 71, (2009). Abstract
Long-term variation in TOMS ozone over 60 deg.-70 deg. S. Geophysical Research Letters 24, 2295-2298 (1997).
On the exploitation of polarimetric ratio for oil spill detection. Electronic proceedings (EUSAR) 2016:7559371, (2016).
Atmospheric planetary boundary layer (ABL/PBL). Part II: The role of large, organised eddies in the convective heat/mass transfer. Atmospheric boundary layer flows in air pollution modelling , VKI LS 2008-06, D/208/0238/526, 2.1-2.6 (2008).
The effect of stratification on the surface resistance for very rough vegetated and urban surfaces. Sixth International Conference on Urban Climate 415-418 (2006).
On the velocity gradient in the stably stratified sheared flows. Part 1: Asymptotic analysis and applications. Boundary-Layer Meteorology 135, (2010). Abstract
Diagnostic and prognostic equations for the depth of the stably stratified Ekman boundary layer. Quarterly J. Royal Meteorol. Soc. 25-46 (2002).
Monitoring and forecasting of personal environment. Fundamentalnaya i prikladnaya gidrofizika 9, (2016).
Similarity theory and calculation of turbulent fluxes at the surface for the stably stratified atmospheric boundary layer. Atmospheric Boundary Layers: Nature, Theory and Applications to Environmental Modelling and Security 37-49 (2007).på <http://www.springerlink.com.pva.uib.no/content/978-0-387-74318-9/#section=167162&page=3&locus=29> Abstract
Atmospheric planetary boundary layer (ABL/PBL). Part I: Stably stratified atmospheric boundary layer (SBL). Atmospheric boundary layer flows in air pollution modelling , VKI LS 2008-06 (ed. by J.P.A. van Beek, J.-M. Buchlin, A. Petrosyan), von Karman Institute for Fluid Dynamics, ISBN-13 978-2-930389-85-0, D/208/0238/526, 1.1-1.15 (2008).
Turbulent energetics in the stably stratified geophysical flows and the problem of critical Richardson number. International Conference Mesoscale Meteorology and Air Pollution in Commemoration of the Late Professor Lev Gutman and His Outstanding Contribution to Theoretical Mesometeorology, 15-17 September 2008, Odessa State Environmental University, Odessa, Ukra (2008).
Modeling stable boundary layers (key lecture). SABLE Workshop. Abstracts and Presentations, November 12 - 16, 2006 (2006).
Principal comments on numerical simulation of homogeneous stably stratified turbulence. Boundary-Layer Meteorology (2010).doi:10.1007/s10546-010-9484-1
The effect of baroclinicity on the depth of neutral and stable planetary boundary layers. Quart, J. Roy. Met. Soc. 3339-3356 (2003).
What do we need from experiments to better model physical processes in stable boundary layers?. CD-ROM Sodankylä Seminar on Stable Boundary Layers. Sodankylä, Finland, 30-31 August 2004, Finnish Meteorological Institute. (2004).
The effect of stratification on the roughness length and displacement height. ICTP Fall Colloquium on the Physics of Weather and Climate: Regional Weather Predictability and Modelling, Trieste, Italy, 29 September 10 October 2008. Abstract: the Colloquium web site (2008).
On integral measures of the neutral, barotropic planetary boundary layers. Boundary-layer Meteorology 371-379 (2002).på <http://www.springerlink.com/content/100245/?p=43e84a3972f3443fbe3e13aeb2578da0&pi=0>
Atmospheric planetary boundary layer feedback in climate system and triggering of climate change at high latitudes. EGU General Assembly 11, (2009).
